Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 14
... respectively , until its total submergence and transgression both in Zanskar and Chamba - Tandi areas from Permian onwards . This uplift and erosion is evident from the absence of over 5 km of late Precambrian to early Permian sediments ...
... respectively , until its total submergence and transgression both in Zanskar and Chamba - Tandi areas from Permian onwards . This uplift and erosion is evident from the absence of over 5 km of late Precambrian to early Permian sediments ...
Page 182
... respectively . Oo , o are the initial ray take off angle and azimuth and Io , Qo , o are the unit vectors along the P , SV , and SH wave directions respectively . 2 2 1/2 i · v2 ; p2 ) 2 + 1 ) / ( ( 1 − ( v ; + a ̧ h ” ) 2 p2 + 1 ) ...
... respectively . Oo , o are the initial ray take off angle and azimuth and Io , Qo , o are the unit vectors along the P , SV , and SH wave directions respectively . 2 2 1/2 i · v2 ; p2 ) 2 + 1 ) / ( ( 1 − ( v ; + a ̧ h ” ) 2 p2 + 1 ) ...
Page 185
... respectively . The matrix inversion can be replaced by an iterative scheme due Zeng ( 1991 ) . Under the assumption that model and noise vectors obey joint Gaussian distribution , the following set of recursive equations are obtained ...
... respectively . The matrix inversion can be replaced by an iterative scheme due Zeng ( 1991 ) . Under the assumption that model and noise vectors obey joint Gaussian distribution , the following set of recursive equations are obtained ...
Contents
CHOUBEY Kewal K Sharma D RAMESHWAR RAO Crustal anatexis | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 9 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 11 |
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02:53 IST MAGNITUDE Accel cm/s² Agglomeratic Slate Amritpur axial plane Bafliaz Formation basin biotite Budhal Burtsa Formation calcite chert clasts conglomerate Cretaceous deformation Dehra Dun deposits dolomite Dum Gali Quartzite facies fault plane feldspar folds foliation fossils Garhwal Geol gneiss grained granites granitoids grey Gulabgarh Himachal Himalaya Himalayan Geology India Infrakrol Institute of Himalayan inversion Jour Jutogh Kashmir Kharnak Krol Ladakh landslides Lesser Himalaya limestone lineation Maastrichtian Mandi metamorphic Nappe Nilkanth Panjal thrust Panjal Volcanic Parautochthonous belt pebbles periglacial Permian phyllites Pir Panjal range plagioclase porphyries Proterozoic quartz quartzite Rampur Ramsu region rocks Salkhala samples sandstone Sarkanth schist sector sedimentary sediments sequence shale Sharma shear Shergol Singh SiO2 slide slip slope soil strain Stratigraphy structures Surv Suture Zone Syncline tectonic Tethyan Thakur thick Thinly bedded Uhl valley Unconformity upper UTTARKASHI UTTARKASHI EARTHQUAKE Verma Wadia Institute WIMF/A Ypresian Zanskar